Sea-breeze thunderstorms are anticipated in coastal regions due to the differential heating between land and sea, leading to a convergence of air masses. During the day, the land heats up faster than the sea, creating a pressure gradient that causes a sea breeze to blow inland. This convergence can lead to the formation of cumulus clouds, which, in unstable atmospheric conditions, develop into thunderstorms. These thunderstorms often intensify near the convergence zone, posing hazards such as flash flooding from heavy rainfall and property damage from gusty winds. Lightning strikes also present a significant risk, necessitating safety precautions. Coastal communities should stay informed about weather forecasts and warnings, taking appropriate measures to protect themselves and their property.